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Modeling Fluid Flow in Faulted Basins

机译:模拟断陷盆地中的流体

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Modeling Fluid Flow in Faulted Basins — This paper presents a basin simulator designed to better take faults into account, either as conduits or as barriers to fluid flow. It computes hydrocarbon generation, fluid flow and heat transfer on the 4D (space and time) geometry obtained by 3D volume restoration. Contrary to classical basin simulators, this calculator does not require a structured mesh based on vertical pillars nor a multi-block structure associated to the fault network. The mesh follows the sediments during the evolution of the basin. It deforms continuously with respect to time to account for sedimentation, erosion, compaction and kinematic displacements. The simulation domain is structured in layers, in order to handle properly the corresponding heterogeneities and to follow the sedimentation processes (thickening of the layers). In each layer, the mesh is unstructured: it may include several types of cells such as tetrahedra, hexahedra, pyramid, prism, etc. However, a mesh composed mainly of hexahedra is preferred as they are well suited to the layered structure of the basin. Faults are handled as internal boundaries across which the mesh is non-matching. Different models are proposed for fault behavior such as impervious fault, flow across fault or conductive fault. The calculator is based on a cell centered Finite Volume discretisation, which ensures conservation of physical quantities (mass of fluid, heat) at a discrete level and which accounts properly for heterogeneities. The numerical scheme handles the non matching meshes and guaranties appropriate connection of cells across faults. Results on a synthetic basin demonstrate the capabilities of this new simulator.
机译:为断层盆地中的流体流动建模—本文提出了一种盆地模拟器,旨在更好地考虑断层,将其作为导管或流体流动的障碍。它通过3D体积还原获得的4D(空间和时间)几何计算碳氢化合物的生成,流体流动和热传递。与经典的盆地模拟器相反,该计算器不需要基于垂直支柱的结构化网格,也不需要与断层网络关联的多块结构。网格在盆地演化过程中跟随沉积物。它会随时间连续变形,以解决沉降,侵蚀,压实和运动位移。模拟域是分层结构的,以便正确处理相应的异质性并遵循沉积过程(各层的厚度)。在每一层中,网格都是非结构化的:它可以包含几种类型的单元,例如四面体,六面体,金字塔,棱柱等。但是,主要由六面体组成的网格是优选的,因为它们非常适合盆地的分层结构。断层被处理为网格不匹配的内部边界。针对故障行为提出了不同的模型,例如渗透性故障,跨故障流或导电性故障。该计算器基于以单元为中心的有限体积离散化,该离散化可确保在离散水平上保留物理量(流体质量,热量),并适当考虑了异质性。数值方案处理不匹配的网格,并保证跨断层的单元的适当连接。合成盆上的结果证明了这种新模拟器的功能。

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